Scaling properties of heavy rainfall at short duration: A regional analysis

被引:29
作者
Ceresetti, D. [1 ]
Molinie, G. [1 ]
Creutin, J. -D. [1 ]
机构
[1] Univ Grenoble, CNRS, Lab Etude Transfert Hydrol & Environm, INPG,IRD,UJF, F-38041 Grenoble 9, France
关键词
SPATIAL RAINFALL; PRECIPITATING EVENTS; FRANCE; MODEL; MULTIFRACTALS; FRAMEWORK;
D O I
10.1029/2009WR008603
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The aim of this paper is to assess the scaling properties of heavy point rainfall with respect to duration. In the region of interest, the probability distribution tails of hourly to daily rainfall display log-log linearity. The log-log linearity of tails is a feature of fat-tailed distributions. The conservation of this property throughout the scales will be investigated in the framework of scale-invariant analysis. Evidence of the scaling of heavy rainfall is shown for one particularly long rainfall series through the conservation of the survival probability shape at durations in the range 1-24 h. An objective method is implemented to estimate the hyperbolic-tail parameters of rainfall distributions. This method is automatized and detects the lower bound above which the distributions exhibit power law tails and determines the power law exponent a using a maximum likelihood estimator. The application of unbiased estimation methods and scale-invariant properties for the estimation of the power law exponent provides a significant reduction of the intergage power law variability. This achievement is essential for a correct use of geostatistical approaches to interpolate the power law parameters at ungaged sites. The method is then applied to the rain gage network in the Cevennes-Vivarais region, a Mediterranean mountainous region located in southern France. The maps show thicker rainfall distribution tails in the flat area between the seashore and the foothill. It is shown that in a flat region closer to the Mediterranean Sea the rainfall distribution tails are hyperbolic and the power law exponent is quasi-constant with duration, whereas, over the mountain, the power law behavior is less defined. The physical reasons for such results and the consequences for the statistical modeling of heavy rainfall are then discussed, providing an innovative point of view for the comprehension of the rainfall extremes behavior at different temporal scales.
引用
收藏
页数:12
相关论文
共 41 条
[1]  
[Anonymous], 2004, Critical Phenomena in Natural Sciences: Chaos, Fractals Selforganization and Disorder: Concepts and Tools
[2]  
BENDJOUDI H, 1997, C R ACAD SCI 2A, V2, P323
[3]   Regional rainfall depth-duration-frequency equations for an alpine region [J].
Borga, M ;
Vezzani, C ;
Dalla Fontana, G .
NATURAL HAZARDS, 2005, 36 (1-2) :221-235
[4]   Scaling and multiscaling models of depth-duration-frequency curves for storm precipitation [J].
Burlando, P ;
Rosso, R .
JOURNAL OF HYDROLOGY, 1996, 187 (1-2) :45-64
[5]   Stochastic model for generating hourly hyetographs [J].
Cernesson, F ;
Lavabre, J ;
Masson, JM .
ATMOSPHERIC RESEARCH, 1996, 42 (1-4) :149-161
[6]  
Chiles Jean-Paul, 2009, Geostatistics: Modeling Spatial Uncertainty, V497
[7]   Power-Law Distributions in Empirical Data [J].
Clauset, Aaron ;
Shalizi, Cosma Rohilla ;
Newman, M. E. J. .
SIAM REVIEW, 2009, 51 (04) :661-703
[8]   The catastrophic flash-flood event of 8-9 September 2002 in the Gard region, France:: A first case study for the Cevennes-Vivarais Mediterranean Hydrometeorological Observatory [J].
Delrieu, G ;
Ducrocq, V ;
Gaume, E ;
Nicol, J ;
Payrastre, O ;
Yates, E ;
Kirstetter, PE ;
Andrieu, H ;
Ayral, PA ;
Bouvier, C ;
Creutin, JD ;
Livet, M ;
Anquetin, S ;
Lang, M ;
Neppel, L ;
Obled, C ;
Parent-du-Châtelet, J ;
Saulnier, GM ;
Walpersdorf, A ;
Wobrock, W .
JOURNAL OF HYDROMETEOROLOGY, 2005, 6 (01) :34-52
[9]  
Delrieu G., 2004, HOUILLE BLANCHE, V6, P83
[10]  
Ducrocq V, 2002, WEATHER FORECAST, V17, P1236, DOI 10.1175/1520-0434(2002)017<1236:SSNRPF>2.0.CO